Abstract
The nature of changes of the parameters of microseismic emission signals (MSE) contains important information about the stage of the deformation process during the destruction of rocks under various types of loading, and can also give predictive estimates of the destruction of the massif. In this paper, the study of the MSE behavior is carried out signals under direct shear loading of samples from tuff sandstone, siltstone and clay crust weathering. The analysis of changes of the parameters of the MSE signals: the number, amplitude of acceleration and frequency at the pre-limit stage, the limit load and the post-peak stage of deformation is given.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: IOP Conference Series: Earth and Environmental Science
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
